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(Table 1e) Chemistry and structural formulae from corrensites of ODP Site 135...
Numbers of cations on the basis of O10(OH)5 -
(Table 1c) Chemistry and structural formulae from trioctahedral smectites of ...
Numbers of cations on the basis of O10(OH)2 -
(Table 1b) Chemistry and structural formulae from dioctahedral illites of ODP...
Numbers of cations on the basis of O10(OH)2 -
(Table 1a) Chemistry and structural formulae from dioctahedral smectites and ...
Numbers of cations on the basis of O10(OH)2 -
NEEM Calcium and Sodium concentrations (10 year averages, 10-60ka BP
This dataset has no description
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NEEM high resolution calcium and sodium concentration (over warming events, 1...
This dataset has no description
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High resolution aerosol records over the past 3.8ka from the EastGRIP ice cor...
High resolution aerosol data from Greenland EastGRIP ice core over the past 3800 years. All data was measured using continuous flow analysis with the Bern CFA system at the... -
Chemical composition of bottom sediments from Hole AMIGE-1993-165 drilled in ...
This dataset has no description
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Element concentrations of amphiboles in ODP Hole 147-894G (Table 1)
Metamorphosed oceanic gabbros provide a record of the cooling history of the lower crust near mid-ocean ridges, but the temperature range, rate, and location of subsolidus... -
Table 1: Soil chemical properties of the analysed depth profiles in the Venic...
Visual traces of iron reduction and oxidation are linked to the redox status of soils and have been used to characterise the quality of agricultural soils.We tested whether this... -
Elemental abundances in marine carbonates from ODP Leg 115 holes (Table 1)
We subjected 18 carbonate samples <1-46 Ma in age from Holes 706A, 707A, 708A, 709C, 710A, and 711A on or near the Mascarene Plateau and Madingley Rise and from Holes 712A,... -
Tab. 1+2: Representative electron-microprobe analyses of minerals from Du Toi...
An example of cordierite-bearing gneiss that is part of a high-grade gneiss-migmatite sequence is described from the Hatch Plain in the Read Mountains of the Shackleton Range,... -
(Table 1) Sediment chemistry and Sulphur isotope ratios of ODP Site 127-795
Sixty sediment samples collected every 10 m from Holes 795A and 795B in the northern Japan Sea were analyzed for 27 major and trace elements using instrumental neutron... -
(Table 1) Geochemistry of ODP Hole 128-798B
Because of heterogeneity, average values of sediment composition can be difficult to establish accurately in fine-grained rocks. As a result, derived values (such as biogenic... -
(Table 1) Geochemistry of ODP Hole 130-807C carbonates across the K/T boundary
Paleontological, stable isotopic, trace elemental abundance, and magnetostratigraphic studies have been performed on limestones spanning the Cretaceous/Tertiary boundary... -
(Tables 2-7) Soil characteristics and geochemistry of marshland in the North ...
Results from a large scale soil mapping on the North Frisian mainland indicate, that field characteristics, particularly the grain-size, bedding, and degree of compaction, with... -
(Table T1) Geochemical composition of coastal sediments from the Schleswig-Ho...
Approximately quantitative values are presented on the mineral content of the clay and silt fractions of marine sediments from the Wadden Sea. Considering the extent of clay... -
(Table T1) Cation exchange capacities and contribution of cations to CEC in s...
Fluid circulation at midocean ridge flank areas where the igneous crust is young and still hot and sediment cover is usually thin actually produces a major chemical exchange... -
(Table 1) Determined and theoretical chemical composition of thaumasite of OD...
Hole 841B was drilled in the forearc region of the Lau Basin at a water depth of 4810 m. The hole penetrated a roughly 500-m-thick series of Miocene volcanic sediments with a... -
(Appendix B) Carbonate fraction geochemistry at DSDP Hole 72-516F
This paper presents data on trace elements (Sr, Mg, Na, K, Mn, Fe, Ni, Cr) and isotopes (13C, 18O) on the carbonate fraction of bulk sediments from the Coniacian to Paleocene...
